987 resultados para Einhard, ca. 770-840.
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.
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La base y objetivo de este estudio es considerar y valorar cada una de las partes del Bildung, desde su inicio hasta su esplendor. Utilizar el concepto de Bildung en las diferentes ciencias: Filosofía, Pedagogía, Psicología, etc. para entender mejor la teoría neohumanista dentro de este mútiple marco. Tratar la proyección pedagógica y los medios o acciones por las cuales el Bildung teórico se convierte en acción. El concepto e historia del Bildung. La investigación realizada ha sido teórica siguiendo el método histórico hermenéutico. Este método se presentó como el más adecuado para estudiar este proceso y su proyección pedagógica. Surgieron dificultades ya que la mayoría de fuentes bibliográficas estaban en el país de origen, muchas eran consideradas reservas bibliográficas y su impresión era en alemán gótico. Finalmente se limitó su marco geográfico a Prusia. Con este trabajo se concluye que el sistema escolar alemán de la época que lo ocupa se basaba en un sistema escolar primario que se terminaba con la Universidad. El trabajo formativo constituía una función regular del cuerpo social, se apoyaba en el Derecho público y era sostenido por el interés general, trabajando por la evolución intelectual de los hombres y elevando gradualmente los diversos niveles en que ésta se realizaba. Una enseñanza multiforme que favorecía su desarrollo en beneficio de la sociedad.
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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
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This layer is a georeferenced raster image of the historic paper map entitled: Map of the town of Northbridge, by Cushing & Walling. It was published by W. Sharp in 1849. Scale [ca. 15,840]. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Massachusetts State Plane Coordinate System, Mainland Zone (in Feet) (Fipszone 2001). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, or other information associated with the principal map. This map shows features such as roads, railroads, drainage, public buildings, schools, churches, cemeteries, industry locations (e.g. mills, factories, mines, etc.), private buildings with names of property owners, town and town district boundaries and more. Relief is shown by hachures. Includes inset: A plan of Whitinsville. Scale [ca. 1:6,030]. This layer is part of a selection of digitally scanned and georeferenced historic maps of Massachusetts from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of regions, originators, ground condition dates (1755-1922), scales, and purposes. The digitized selection includes maps of: the state, Massachusetts counties, town surveys, coastal features, real property, parks, cemeteries, railroads, roads, public works projects, etc.
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Mode of access: Internet.
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Raman spectra of natrouranospinite complemented with infrared spectra were studied and related to the structure of the mineral. Observed bands were assigned to the stretching and bending vibrations of (UO2)2+ and (AsO4)3- units and of water molecules. U-O bond lengths in uranyl and O-H…O hydrogen bond lengths were calculated from the Raman and infrared spectra.
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Raman spectra of metauranospinite Ca[(UO2)(AsO4)]2.8H2O complemented with infrared spectra were studied. Observed bands were assigned to the stretching and bending vibrations of (UO2)2+ and (AsO4)3- units and of water molecules. U-O bond lengths in uranyl and O-H…O hydrogen bond lengths were calculated from the Raman and infrared spectra.
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The mineral lewisite, (Ca,Fe,Na)2(Sb,Ti)2O6(O,OH)7 an antimony bearing mineral has been studied by Raman spectroscopy. A comparison is made with the Raman spectra of other minerals including bindheimite, stibiconite and roméite. The mineral lewisite is characterised by an intense sharp band at 517 cm-1 with a shoulder at 507 cm-1 assigned to SbO stretching modes. Raman bands of medium intensity for lewisite are observed at 300, 356 and 400 cm-1. These bands are attributed to OSbO bending vibrations. Raman bands in the OH stretching region are observed at 3200, 3328, 3471 cm-1 with a distinct shoulder at 3542 cm-1. The latter is assigned to the stretching vibration of OH units. The first three bands are attributed to water stretching vibrations. The observation of bands in the 3200 to 3500 cm-1 region suggests that water is involved in the lewisite structure. If this is the case then the formula may be better written as Ca, Fe2+, Na)2(Sb, Ti)2(O,OH)7 •xH2O.